You can find on this page the Qatar satellite map to print and to download in PDF. The Qatar map from satellite presents new pictures of Qatar as seen from the sky in Western Asia.
The Qatar satellite map shows new pictures of Qatar as seen from the sky. This satellite map of Qatar will allow you to visit the country Qatar in Western Asia as seen from the sky. The Qatar satellite map is downloadable in PDF, printable and free.
satellite view and the map shows Qatar, officially the State of Qatar, an Arab country in the Middle East that occupies a peninsula on the western coast of Arabia. Qatar is geographically closely related to the United Arab Emirates (UAE) and Kuwait. Its interior consists of undulating desert plains and salt flats. In the south it reaches its highest point at the Qurayn Abu al-Bawl (Qurain Abul Bul), at 103 metres above sea level as you can see in Qatar satellite map.
The small (sub)peninsula of Qatar is about 160 kilometres in length and between 55 and 90 kilometres in width. Its total land surface measures 11,437 square kilometres. Qatar’s coastline along the Persian Gulf is 563 kilometres long as its shown in Qatar satellite map. The land border with Saudi Arabia in the south measures 60 kilometres. Much of the central part of the peninsula is formed of a plateau which is composed of limestone and dolomites overlain by up to a few centimetres of broken material.
The State of Qatar lies in the middle of the western coast of the Arabian Gulf between 24° 27' -26° 1 0' N and 50° 45'-51 o 40 ' E with an area of about 11 ,600 Km2 • The Qatar peninsula is composed of Lower Eocene Limestone and gypsum rocks (Cavelier 1970, De Cardi, 1978). The surface of the Qatar peninsula is of low to moderate relief, with the highest elevation of 103 m above sea level being attained in Southern Qatar where mesa type hills and large barchan sand dunes are found as its mentioned in Qatar satellite map (Johnstone and Wilkinson, 1960; FAO, 1981; Eccleston 1982). The Qatar peninsula landscape is dotted by some 2000 depressions of young colluvial deposits of limestone origin which resulted primarily from structural collapse at depth (Halcrow-Balfour, 1981 ).